000 | 03540nam a22005055i 4500 | ||
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001 | 978-90-481-2433-6 | ||
003 | DE-He213 | ||
005 | 20201213204215.0 | ||
007 | cr nn 008mamaa | ||
008 | 100301s2009 ne | s |||| 0|eng d | ||
020 |
_a9789048124336 _9978-90-481-2433-6 |
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024 | 7 |
_a10.1007/978-90-481-2433-6 _2doi |
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050 | 4 | _aTA357-359 | |
072 | 7 |
_aTGMF _2bicssc |
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072 | 7 |
_aTGMF1 _2bicssc |
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072 | 7 |
_aTEC009070 _2bisacsh |
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072 | 7 |
_aSCI085000 _2bisacsh |
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082 | 0 | 4 |
_a620.1064 _223 |
100 | 1 |
_aZeytounian, R. Kh. _eauthor. |
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245 | 1 | 0 |
_aConvection in Fluids _h[electronic resource] / _cby R. Kh. Zeytounian. |
264 | 1 |
_aDordrecht : _bSpringer Netherlands, _c2009. |
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300 |
_aXV, 396 p. _bonline resource. |
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336 |
_atext _btxt _2rdacontent |
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337 |
_acomputer _bc _2rdamedia |
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338 |
_aonline resource _bcr _2rdacarrier |
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347 |
_atext file _bPDF _2rda |
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490 | 1 |
_aFluid Mechanics and its Applications, _x0926-5112 ; _v90 |
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505 | 0 | _aShort Preliminary Comments and Summary of Chapters 2 to 10 -- The Navier—Stokes—Fourier System of Equations and Conditions -- The Simple Rayleigh (1916) Thermal Convection Problem -- The Bénard (1900, 1901) Convection Problem, Heated from below -- The Rayleigh—Bénard Shallow Thermal Convection Problem -- The Deep Thermal Convection Problem -- The Thermocapillary, Marangoni, Convection Problem -- Summing Up the Three Significant Models Related with the Bénard Convection Problem -- Some Atmospheric Thermal Convection Problems -- Miscellaneous: Various Convection Model Problems. | |
520 | _aIn the present monograph, entirely devoted to “Convection in Fluids”, the purpose is to present a unified rational approach of various convective phenomena in fluids (mainly considered as a thermally perfect gas or an expansible liquid), where the main driving mechanism is the buoyancy force (Archimedean thrust) or temperature-dependent surface tension in homogeneities (Marangoni effect). Also, the general mathematical formulation (for instance, in the Bénard problem - heated from below)and the effect of the free surface deformation are taken into account. In the case of the atmospheric thermal convection, the Coriolis force and stratification effects are also considered. The main motivation is to give a rational, analytical, analysis of main above mentioned physical effects in each case, on the basis of the full unsteady Navier-Stokes and Fourier (NS-F) equations - for a Newtonian compressible viscous and heat-conducting fluid - coupled with the associated initiales (at initial time), boundary (lower-at the solid plane) and free surface (upper-in contact with ambiant air) conditions. This, obviously, is not an easy but a necessary task if we have in mind a rational modelling process with a view of a numerical coherent simulation on a high speed computer. | ||
650 | 0 | _aEngineering. | |
650 | 0 | _aMathematics. | |
650 | 0 | _aHydraulic engineering. | |
650 | 1 | 4 | _aEngineering. |
650 | 2 | 4 | _aEngineering Fluid Dynamics. |
650 | 2 | 4 | _aEngineering Thermodynamics, Heat and Mass Transfer. |
650 | 2 | 4 | _aMathematical Modeling and Industrial Mathematics. |
650 | 2 | 4 | _aApplications of Mathematics. |
710 | 2 | _aSpringerLink (Online service) | |
773 | 0 | _tSpringer eBooks | |
776 | 0 | 8 |
_iPrinted edition: _z9789048124329 |
830 | 0 |
_aFluid Mechanics and its Applications, _x0926-5112 ; _v90 |
|
856 | 4 | 0 | _uhttp://dx.doi.org/10.1007/978-90-481-2433-6 |
912 | _aZDB-2-ENG | ||
950 | _aEngineering (Springer-11647) | ||
999 |
_c24534 _d24534 |